Aquitard: Difference between revisions
Jump to navigation
Jump to search
imported>Anthony Argyriou (spelling) |
imported>Joe Quick m (subpages) |
||
| Line 1: | Line 1: | ||
{{Subpages}} | |||
An '''aquitard''' or '''aquiclude''' is a zone of earth material that will hold water but not transmit it at a useful rate or fast enough to be pumped from a well. Aquitards often form a confining layer through which little water moves. Clay soils, shale, and igneous or metamorphic rocks with little interconnected [[porosity]] or [[Permeability (fluid)|fractures]] are likely to form aquitards. | An '''aquitard''' or '''aquiclude''' is a zone of earth material that will hold water but not transmit it at a useful rate or fast enough to be pumped from a well. Aquitards often form a confining layer through which little water moves. Clay soils, shale, and igneous or metamorphic rocks with little interconnected [[porosity]] or [[Permeability (fluid)|fractures]] are likely to form aquitards. | ||
Revision as of 22:17, 20 December 2007
An aquitard or aquiclude is a zone of earth material that will hold water but not transmit it at a useful rate or fast enough to be pumped from a well. Aquitards often form a confining layer through which little water moves. Clay soils, shale, and igneous or metamorphic rocks with little interconnected porosity or fractures are likely to form aquitards.